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Defining soil sample preparation requirements for MIR spectroscopic analysis using principal components

机译:使用主要成分定义MIR光谱分析的土壤样品制备要求

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Diffuse reflectance MIR (mid-infrared) spectroscopy when combined with PLS (partial lest squares) statistical analyses can be used to quantify various soil chemical properties. Of particular interest is the application of MIR/PLS analysis to provide arapid and cost-effective methodology for predicting soil organic carbon content and its allocation to component fractions for use in soil carbon scenario modelling. The technique applies a beam of approximately 3.14 mm2 (2 mm diameter circle) to the surface of a powdered soil sample to define chemical composition. Given the small area sampled, soil sample homogeneity and particle size become important issues to examine when interpreting the spectral results obtained. MIR analysis was completed on threedifferent soils with variable texture that had been ground for durations ranging from 0-180s, Four aliquots of four replicate samples prepared for each soil by grinding time combination were analysed. Principal components analysis (PCA) was applied to the acquired MIR spectra to define to spectral variability and PLS analysis of the spectra was used to quantify the variability in predicted values for soil carbon and carbon fraction contents. PCA provided an excellent means of assessing the impact of grinding on the spectral homogeneity for each of the soils examined. The sandy soil required significantly more grinding time to reduce the variability of acquired MIR spectra. However the variability in predicted organic carbon and carbon fraction contents stabilised at shorter grinding times.
机译:弥散反射miR(中红外)光谱在与PLS(部分自由方)结合时统计分析可用于量化各种土壤化学性质。特别令人兴趣的是施用miR / pls分析,提供Arapid和成本效益的方法,用于预测土壤有机碳含量及其对组分级分的分配,用于土壤碳情景建模。该技术将大约3.14mm 2(直径圆圈)的光束施加到粉末状土样品的表面上以定义化学成分。考虑到小区采样,土壤样本均匀性和粒度是在解释所获得的光谱结果时检查的重要问题。在具有0-180秒的持续时间的耐脉冲纹理的可变纹理上完成了MIR分析,分析了通过研磨时间组合为每种土壤制备的四个重复样品的四个等分试样。将主成分分析(PCA)应用于所获得的MIR光谱,以定义光谱变异性,并且光谱的PLS分析用于量化土壤碳和碳馏分含量的预测值的可变性。 PCA提供了一种评估研磨对所检查各土壤的光谱均匀性的影响的优异方法。砂土需要显着更大的研磨时间来降低获得的MIR光谱的可变性。然而,预测有机碳和碳馏分含量的可变性在较短的研磨时间下稳定。

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